Titlebook: Climatic Variability in Sixteenth-Century Europe and Its Social Dimension; Christian Pfister,Rudolf Brázdil,Rüdiger Glaser Book 1999 Sprin

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預(yù)感

James R. Pinnells,Eleanor Pinnellspresented and classified in this article and then further analyzed in subsequent papers included in this volume. The sixteenth century witnessed an increase in the number and variety of sources in Switzerland, Germany and the Czech Republic as well as in the western and northern parts of ancient Hun

Inclement

https://doi.org/10.1007/978-3-322-81239-1ed. Systematic weather observations were promoted by the rise of planetary astronomy and its application in astro-meteorology. The practice of keeping weather diaries spread from Cracow (Poland) to Ingolstadt (Germany) and from there to other universities. The data obtained from these sources provid

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高歌

Karin Reisinger,Helmut Pernsteiner Germany, the Czech Republic, northern Italy, ancient Hungary, Poland and Spain). Besides methodological aspects about the formation of indices, especially the progress as well as the question of similarity development of these series in the 16th century are discussed and shown on the balance sheet.

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Cupidity

Risikomanagement in Unternehmentorical sources, as well as dendrochronological investigations of larches that were destroyed by glacier advances (Great Aletsch Glacier), have shed much light in recent years on glacial movements in the 16th century. Many of the earliest know Records for glacial activity in the Western Alps date fr

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